Lithium isotope behavior under extreme tropical weathering: A case study of basalts from the Hainan Island, South China

Abstract

Chemical weathering of silicate rocks (especially basalt) is an important sink of atmospheric carbon dioxide, and has an important impact on long-term carbon cycle and storage. Lithium (Li) isotopes have been regarded as a good tracer of chemical weathering, however, the behavior of Li isotopes in tropical settings is poorly understood. In this study, we studied the Li elemental and isotopic variation in the solid weathering products (soil and saprolite) from a highly-weathered (CIA ∼100%) basalt weathering profile (>15 m thick, including soil, saprolite, semi-weathered rock and fresh basalt) on the tropical Hainan Island in South China. The weathering products have 1.99–58.1 ppm Li, mostly below the average fresh basalt value (4.6 ppm, n = 5). The δ7Li values (−14.3 to 8.9‰) of the solid weathering products exhibit complex stratigraphic variation across the weathering profile. The Li and Mn enrichments coincide spatially, with the Mn-rich samples having the highest Li content and lowest δ7Li value. Lithium is enriched in the semi-weathered basalt sample, but its δ7Li value (−2.7‰) is close to that of fresh basalts (0.7–5.3‰, avg. 3.0‰, n = 5). Strontium isotope data show that the weathering profile is affected by marine aerosol input, and the marine strontium may have been leached to the profile bottom or out of it under extreme weathering. Sequential extraction results indicate that Li in the soil, saprolites (lower part), and semi-weathered basalt occurs mainly in the residual phase, while Li in the saprolites (middle part) occurs largely in Fe–Mn oxides. We suggest that Li isotope fractionation in the upper, middle and lower parts of the profile was controlled by, respectively, marine aerosol input and secondary mineral leaching, dissolution/re-precipitation of Fe–Mn oxides, and neoformation of secondary minerals from heavy pore water. Our results show that the preferential light Li isotope uptake by Fe–Mn oxides may have been the main cause for the major Li isotope fractionation in the Wenchang weathering profile.